# Comparison of published versus recalibrated age models for Makassar Strait Core 2160, Indonesia #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/21731 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/pages2k/dixon2017australasia/dixon2017md2160.txt # Description: NOAA location of the template # # Original_Source_URL: http://hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:::::P1_STUDY_ID:5534 # Description: # # Archive: Foraminifera d18O, Mg/Ca # # Parameter_Keywords: #--------------------------------------- # Contribution_Date # Date: 2017-12-12 #--------------------------------------- # File_Last_Modified_Date # Date: 2017-12-12 #--------------------------------------- # Title # Study_Name: Comparison of published versus recalibrated age models for Makassar Strait Core 2160, Indonesia #--------------------------------------- # Investigators # Investigators: Dixon, Bronwyn C.; Tyler, Jonathan J.; Lorrey, Andrew M; Goodwin, Ian D; Gergis, Joelle; Drysdale, Russell N #--------------------------------------- # Description_Notes_and_Keywords # Description: # Provided Keywords: age modelling, Bayesian #--------------------------------------- # Publication # Authors: Dixon, Bronwyn C.; Tyler, Jonathan J.; Lorrey, Andrew M; Goodwin, Ian D; Gergis, Joelle; Drysdale, Russell N # Published_Date_or_Year: 2017 # Published_Title: Low-resolution Australasian palaeoclimate records of the last 2000 years # Journal_Name: Climate of the Past # Volume: # Edition: # Issue: # Pages: # Report Number: # DOI: # Online_Resource: # Full_Citation: # Abstract: Non-annually resolved palaeoclimate records in the Australasian region were compiled to facilitate investigations of decadal to centennial climate variability over the past 2000 years. A total of 661 lake/wetland, geomorphic, marine, and speleothem records were identified and then assessed against a set of a priori criteria based on temporal resolution, record length, dating methods, and confidence of the proxy-climate relationship over the Common Era. A high quality subset of 22 records across Australasia met the criteria and they are endorsed for subsequent analyses. New chronologies based on progressive Bayesian techniques were constructed for the high quality records to ensure a consistent approach to age modelling and quantification of age uncertainties. Chronological uncertainty was the primary reason why records did not meet the selection criteria. Despite present limitations, existing proxies and reconstruction techniques that successfully capture climate variability in the region show potential to address spatial gaps and expand the range of climate variables covering the last 2000 years from the Australasian region. #--------------------------------------- # Publication # Authors: Newton A; Thunell R; Stott L # Published_Date_or_Year: 2006 # Published_Title: Climate and hydrographic variability in the Indo pacific Warm Pool during the last millennium # Journal_Name: Geophysical Research Letters # Volume: 33 # Edition: # Issue: 19 # Pages: L19710 # Report Number: # DOI: L19710 10.1029/2006gl027234 # Online_Resource: # Full_Citation: Newton, A., Thunell, R. & Stott, L. 2006. Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium. Geophysical Research Letters, 33. # Abstract: Planktonic foraminiferal Mg/Ca and delta(18)O derived sea surface temperature and salinity records from the Makassar Strait, Indonesia, show a long-term cooling and freshening trend, as well as considerable centennial-scale variability during the last millennium. The warmest temperatures and highest salinities occurred during the Medieval Warm Period (MWP), while the coolest temperatures and lowest salinities occurred during the Little Ice Age (LIA). These changes in the western Pacific, along with observations from other high resolution records indicate a regionally coherent southern displacement of the Inter-tropical Convergence Zone during the LIA, with more arid conditions in the northern tropics and wetter conditions in the southern tropics. #--------------------------------------- # Publication # Authors: Geology # Published_Date_or_Year: # Published_Title: 2011 # Journal_Name: 39 # Volume: 1 # Edition: 63-66 # Issue: # Pages: 10.1130/g31421.1 # Report Number: # DOI: The Indonesian Throughflow (ITF) is the only low-latitude conduit for exchange of surface and thermocline waters between the Indian and Pacific Oceans; 80% of the ITF waters pass through the Makassar Strait. The flux of heat and salt through the strait is, in part, a function of the density difference between its southern and northern ends. Here the Mg/Ca and stable oxygen isotope compositions of the planktonic foraminifer Globigerinoides ruber sampled from two sediment cores collected at the northern and southern ends of the Makassar Strait are used to reconstruct surface-water temperature (SST), sea-surface salinity (SSS), and seawater density variability over the past 2000 yr. Maximum SST and SSS occurred at both sites between 850 and 700 yr ago, coinciding with the Medieval Solar Maximum and Medieval Warm Period (ca. 1000-700 yr ago). SST and SSS declined at both locations after 700 yr ago and reached minimum values during the Little Ice Age, between 300 and 100 yr ago. However, the magnitude of SST and SSS change over the past 2000 yr was distinctly different between the two sites, especially during the period between 2000 and 900 yr ago. This led to changes in the south to north density gradient within the Makassar Strait. Specifically, the time interval from ca. 2000 to 800 yr ago was marked predominantly by higher densities at the northern end relative to the southern end of the strait, suggesting reduced heat flux from the Pacific to the Indian Ocean. This is consistent with previous work showing that this time interval was also marked by frequent El Nino conditions. Conversely, the period from ca. 800 to 300 yr ago, including the LIA, was marked by frequent periods when surface density was higher at the southern end of the strait, indicative of enhanced heat flux to the Indian Ocean. # Online_Resource: Newton, A., Thunell, R. & Stott, L. 2011. Changes in the Indonesian Throughflow during the past 2000 yr. Geology, 39, 63-66. # Full_Citation: # Abstract: #--------------------------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #--------------------------------------- # Site Information # Site_Name: Makassar Strait # Location: # Country: # Northernmost_Latitude: -5.2 # Southernmost_Latitude: -5.2 # Easternmost_Longitude: 117.49 # Westernmost_Longitude: 117.49 # Elevation: -1185 #--------------------------------------- # Data_Collection # Collection_Name: MD9821-60 # First_Year: 945.64 # Last_Year: 109.95 # Time_Unit: cal yr BP # Core_Length: 202 # Notes: #--------------------------------------- # Chronology_Information # Chronology: # All dates include a reservoir age of 75 +/- 80 years, Ages from Newton et al. (2011). # Lab ID # Dated material mixed G. Sacculifer and G. ruber mixed G. Sacculifer and G. ruber mixed G. Sacculifer and G. ruber mixed G. Sacculifer and G. ruber mixed G. Sacculifer and G. ruber # depth_bot (mm) NaN NaN NaN NaN NaN # depth_top (mm) 150 360 720 1380 2000 # age (bp) 135 NaN NaN NaN NaN # age14C (bp) NaN 720 1005 1565 2460 # age_error (years) NaN 60 35 40 70 # calibrated age (cal BP) NaN 280 520 1040 1990 # 2-sigma error of cal age (years) NaN NaN NaN NaN NaN # cal_age_range_old (bp) NaN 382 597 947 NaN # cal_age_range_young (2_s) NaN 174 479 1115 NaN # depth (mm) NaN NaN NaN NaN NaN # thickness (mm) NaN NaN NaN NaN NaN # notes tephra 1s age range 1s age range 1s age range 1s age range # #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) ## Depth_cm ,Depth,NA,,cm,NA,NA,,NA,N ## PublishedAge_YBP ,Ages from original record publication,NA,,years before present (present=1950CE),NA,NA,,NA,N ## BACON0.05CI ,5% confidence interval age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),NA,NA,,NA,N ## BACON0.95CI ,95% confidence interval age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),NA,NA,,NA,N ## BACONmedian ,median sample age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),NA,NA,,NA,N ## BACONwmean ,weighted mean age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),NA,NA,,NA,N ## Mg/Ca ,Ratio of Mg to Ca,Globigerinoides ruber ,1s analytical precision >1.0% ,mmol/mol,Jun-Sep,foraminifera,,Inductively Coupled Plasma Atomic Emission Spectrometry,N ## Temperature ,Temperature derived from Mg/Ca measurement,NA,Equation has standard error of 1.2%, (°C),NA,NA,,Mg/Ca = 0.38 exp(0.09T), rearranged to T=((1/0.09)*LN((Mg/Ca)/0.38)),N ## d18Ocalcite ,d18O of foraminifera tests,Globigerinoides ruber ,standard reproducibility ±0.07% ,per mil VPDB,Jun-Sep,foraminifera,,Isotope ratio mass spectrometry,N ## d18Osw (SMOW) ,d18O of seawater, calculated from d18O of foram calcite and calculated seawater temperature,NA,Equation has standard error of 0.5°C,per mil VSMOW,NA,NA,,T(oC) = 14.9 – 4.80(dc – dsw) ,N ## Salinity ,Seawater salinity, calculated from the d18O of seawater,NA,,per mil,NA,NA,,dsw = 0.42S – 14.3 ,N #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NA Core MD98-2160 Depth (cm) Cal YBP Depth_cm PublishedAge_YBP BACON0.05CI BACON0.95CI BACONmedian BACONwmean Mg/Ca Temperature d18Ocalcite d18Osw 0 110 0 110 -25 61 21 21 5.020 28.68 -3.114 0.027 1 112 1 112 -18 67 30 29 5.541 29.78 -3.043 0.326 2 113 2 113 -9 74 38 36 5.315 29.31 -2.999 0.274 3 115 3 115 1 80 46 44 5.118 28.89 NA NA 4 117 4 117 10 87 54 53 5.047 28.74 -2.954 0.199 5 118 5 118 17 92 61 60 NA NA NA NA 6 120 6 120 26 98 68 67 NA NA -3.021 NA 7 122 7 122 36 103 76 75 5.059 28.76 -2.963 0.196 8 123 8 123 43 108 84 82 4.980 28.59 -3.062 0.060 9 125 9 125 55 114 91 90 NA NA NA NA 10 127 10 127 66 120 99 97 4.849 28.29 -2.908 0.153 11 128 11 128 75 125 107 105 4.886 28.38 -2.898 0.180 12 130 12 130 86 129 114 113 NA NA NA NA 13 132 13 132 97 133 122 120 5.033 28.71 NA NA 14 133 14 133 112 136 129 128 NA NA NA NA 15 135 15 135 132 138 135 135 4.820 28.23 -2.988 0.059 16 135 16 135 134 156 140 142 NA NA NA NA 17 135 17 135 137 169 147 149 NA NA NA NA 18 137 18 137 141 181 155 156 4.822 28.23 -2.946 0.102 19 138 19 138 145 190 162 164 5.187 29.04 -2.857 0.360 20 140 20 140 150 202 169 171 5.448 29.59 -3.156 0.174 21 142 21 142 155 210 177 178 5.262 29.20 -2.981 0.269 22 143 22 143 160 220 184 186 4.953 28.53 -2.898 0.212 23 145 23 145 166 228 192 193 5.010 28.66 -3.030 0.106 24 147 24 147 171 238 199 200 5.131 28.92 -2.936 0.255 25 148 25 148 177 246 206 207 5.143 28.95 -3.113 0.084 26 150 26 150 183 256 213 215 4.619 27.75 -3.142 -0.194 27 163 27 163 189 263 220 222 4.588 27.68 -3.123 -0.190 28 176 28 176 194 272 227 229 4.722 28.00 -3.062 -0.063 29 189 29 189 199 281 235 236 4.737 28.03 -2.872 0.134 30 202 30 202 205 289 242 244 4.818 28.22 -2.933 0.113 31 215 31 215 211 297 249 251 4.731 28.02 -3.201 -0.197 32 228 32 228 217 307 256 258 4.850 28.30 -2.970 0.091 33 241 33 241 223 316 264 265 4.566 27.62 -3.176 -0.255 34 254 34 254 229 323 271 273 5.014 28.66 -3.191 -0.053 35 267 35 267 235 333 278 280 4.780 28.13 -3.074 -0.047 36 280 36 280 241 340 286 287 4.932 28.48 -2.886 0.214 37 287 37 287 247 350 293 295 5.038 28.72 -3.020 0.128 38 293 38 293 253 358 300 302 4.696 27.94 -3.007 -0.022 39 300 39 300 259 366 307 309 4.808 28.20 -3.139 -0.098 40 307 40 307 265 373 314 316 4.877 28.36 -3.050 0.023 41 313 41 313 272 382 321 323 4.902 28.41 -2.823 0.262 42 320 42 320 278 389 329 331 5.139 28.94 -2.830 0.365 43 327 43 327 284 399 335 338 5.176 29.02 -3.093 0.118 44 333 44 333 290 407 343 345 5.028 28.70 -2.807 0.337 45 340 45 340 298 414 351 353 4.786 28.15 -2.993 0.037 46 347 46 347 304 421 358 360 5.291 29.26 -3.091 0.171 47 353 47 353 310 429 365 367 4.990 28.61 -3.020 0.106 48 360 48 360 315 437 373 375 5.051 28.75 -2.976 0.178 49 367 49 367 321 449 380 382 5.154 28.97 -3.262 -0.060 50 373 50 373 328 455 387 389 4.842 28.28 -2.941 0.116 51 380 51 380 336 462 395 396 5.254 29.18 -3.122 0.124 52 387 52 387 343 471 401 404 4.898 28.40 NA NA 53 393 53 393 349 477 409 411 4.977 28.58 -2.868 0.253 54 400 54 400 356 487 417 418 5.067 28.78 -2.911 0.251 55 407 55 407 361 496 424 425 4.820 28.23 -2.929 0.117 56 413 56 413 368 504 432 433 4.826 28.24 -3.085 -0.035 57 420 57 420 374 512 438 440 5.120 28.90 -2.936 0.250 58 427 58 427 382 518 446 448 5.206 29.08 -3.229 -0.004 59 433 59 433 389 526 453 455 5.357 29.40 -3.097 0.193 60 440 60 440 396 534 460 463 5.380 29.45 -3.141 0.159 61 447 61 447 402 543 467 470 5.096 28.84 -2.898 0.277 62 453 62 453 408 549 474 477 5.189 29.05 -3.228 -0.011 63 460 63 460 417 557 482 485 4.882 28.37 -2.844 0.232 64 467 64 467 424 564 489 492 4.898 28.40 -3.119 -0.035 65 473 65 473 430 573 497 499 5.028 28.70 -2.684 0.460 66 480 66 480 437 581 504 507 5.028 28.70 -3.168 -0.024 67 487 67 487 445 589 511 514 NA NA -3.080 NA 68 493 68 493 451 598 519 522 5.425 29.54 -2.944 0.376 69 500 69 500 458 606 526 529 5.288 29.26 -2.926 0.334 70 507 70 507 467 613 533 536 NA NA -2.715 NA 71 513 71 513 475 620 540 543 NA NA -2.794 NA 72 520 72 520 481 628 547 551 4.829 28.25 -2.976 0.075 73 528 73 528 488 636 554 558 5.777 30.24 -2.879 NA 74 536 74 536 494 646 562 566 5.390 29.47 -2.908 0.397 75 544 75 544 501 654 570 573 5.228 29.13 -3.004 0.231 76 552 76 552 506 662 577 580 5.150 28.96 -2.918 0.282 77 560 77 560 513 670 584 587 5.164 28.99 -2.913 0.293 78 567 78 567 519 678 591 595 5.018 28.67 -3.078 0.061 79 575 79 575 526 687 599 602 5.553 29.80 -2.893 0.480 80 583 80 583 532 696 606 610 4.965 28.56 -3.037 0.078 81 591 81 591 540 703 615 617 4.945 28.51 -2.923 0.182 82 599 82 599 546 712 622 625 5.460 29.61 -2.934 0.401 83 607 83 607 552 720 629 632 5.152 28.97 -2.729 0.471 84 615 84 615 559 727 637 640 5.056 28.76 -2.708 0.449 85 623 85 623 567 736 644 647 5.378 29.44 -2.879 0.421 86 630 86 630 574 744 651 655 5.158 28.98 -2.837 0.366 87 638 87 638 581 750 658 662 5.072 28.79 -2.857 0.308 88 646 88 646 588 759 666 669 5.284 29.25 -2.821 0.438 89 654 89 654 596 768 673 677 5.194 29.06 -2.911 0.309 90 662 90 662 603 776 681 684 5.090 28.83 -2.813 0.360 91 670 91 670 610 785 689 692 5.076 28.80 -2.825 0.342 92 678 92 678 616 793 696 699 5.266 29.21 -2.972 0.279 93 686 93 686 622 801 704 706 5.150 28.96 NA NA 94 693 94 693 630 810 711 714 NA NA -2.857 NA 95 701 95 701 635 818 718 721 5.760 30.21 -3.012 0.447 96 709 96 709 643 827 725 729 5.386 29.46 -2.971 0.333 97 717 97 717 649 836 733 737 5.501 29.69 -2.828 0.525 98 725 98 725 656 845 740 744 5.494 29.68 -2.862 0.487 99 733 99 733 663 851 749 751 5.519 29.73 -2.754 0.606 100 741 100 741 670 859 756 759 NA NA -2.864 NA 101 749 101 749 677 868 763 767 4.946 28.51 -2.769 0.337 102 757 102 757 684 876 771 774 5.601 29.89 -2.804 0.590 103 764 103 764 691 884 778 781 5.285 29.25 NA NA 104 772 104 772 697 892 785 789 5.435 29.56 -2.758 0.567 105 780 105 780 702 898 793 796 5.384 29.46 -2.904 0.399 106 788 106 788 711 906 800 804 5.231 29.14 -3.176 0.060 107 796 107 796 717 914 809 811 NA NA -2.965 NA 108 804 108 804 726 922 816 819 5.247 29.17 -3.177 0.066 109 812 109 812 732 930 823 826 5.568 29.83 NA NA 110 820 110 820 740 941 830 833 5.601 29.89 -3.149 0.245 111 827 111 827 746 946 837 841 5.222 29.12 -2.684 0.548 112 835 112 835 753 954 845 848 5.133 28.93 -3.275 -0.083 113 843 113 843 761 959 852 856 5.599 29.89 -2.907 0.486 114 851 114 851 767 969 860 863 4.843 28.28 -2.836 0.221 115 859 115 859 773 977 867 871 5.469 29.63 -2.993 0.346 116 867 116 867 780 983 875 878 NA NA NA NA 117 875 117 875 788 992 882 886 5.962 30.59 -3.104 0.434 118 883 118 883 795 1001 891 893 4.970 28.57 -2.983 0.134 119 890 119 890 802 1012 898 900 5.081 28.81 -3.001 0.168 120 898 120 898 808 1019 904 908 5.529 29.75 -2.741 0.623 121 906 121 906 814 1027 912 915 5.723 30.13 -2.922 0.522 122 914 122 914 822 1035 920 923 5.150 28.96 -2.981 0.218 123 922 123 922 828 1042 927 930 5.509 29.71 -2.876 0.480 124 930 124 930 835 1050 934 937 5.436 29.56 -3.142 0.182 125 938 125 938 841 1057 942 945 4.825 28.24 -3.004 0.045 126 946 126 946 850 1064 950 952 5.015 28.67 -2.947 0.191 127 NA 127 NA 857 1072 957 960 NA NA -2.90 128 NA 128 NA 864 1081 964 967 5.68 30.05 -3.21 129 NA 129 NA 872 1089 972 975 5.25 29.176 -3.13 130 NA 130 NA 880 1095 979 983 5.51 29.713 -2.98 131 NA 131 NA 887 1105 987 990 5.38 29.447 NA 132 NA 132 NA 893 1113 995 997 5.29 29.26 -2.77 133 NA 133 NA 901 1121 1002 1005 5.47 29.632 -2.96 134 NA 134 NA 907 1128 1009 1012 5.21 29.091 -2.88 135 NA 135 NA 911 1137 1016 1020 5.19 29.048 -2.86 136 NA 136 NA 920 1144 1023 1027 5.02 28.678 -2.85 137 NA 137 NA 926 1154 1031 1034 5.26 29.197 -2.77 138 NA 138 NA 934 1160 1038 1041 5.60 29.893 -2.87 139 NA 139 NA 941 1168 1045 1049 5.07 28.788 -2.93 140 NA 140 NA 947 1177 1052 1056 5.65 29.992 -3.16 141 NA 141 NA 955 1183 1061 1064 5.29 29.26 -2.88 142 NA 142 NA 961 1190 1068 1071 5.59 29.873 -2.71 143 NA 143 NA 966 1198 1075 1078 5.05 28.744 -2.62 144 NA 144 NA 973 1206 1083 1086 5.33 29.344 -3.02 145 NA 145 NA 980 1216 1090 1093 5.38 29.447 -3.04 146 NA 146 NA 986 1224 1097 1101 5.40 29.489 -2.83 147 NA 147 NA 995 1234 1105 1108 5.41 29.509 -3.06 148 NA 148 NA 1002 1241 1113 1116 NA NA -2.95 149 NA 149 NA 1009 1250 1120 1124 NA NA NA 150 NA 150 NA 1017 1259 1128 1131 5.48 29.652 -3.00 151 NA 151 NA 1025 1267 1136 1139 5.26 29.197 -3.19 152 NA 152 NA 1031 1276 1143 1146 5.30 29.281 -3.11 153 NA 153 NA 1039 1287 1150 1154 5.34 29.365 -3.02 154 NA 154 NA 1045 1294 1158 1161 NA NA NA 155 NA 155 NA 1052 1301 1166 1169 4.98 28.589 -3.08 156 NA 156 NA 1060 1308 1173 1176 5.45 29.591 -3.13 157 NA 157 NA 1065 1316 1180 1183 5.20 29.069 -3.01 158 NA 158 NA 1069 1322 1187 1191 5.20 29.069 -3.34 159 NA 159 NA 1078 1332 1194 1198 5.54 29.773 -3.07 160 NA 160 NA 1083 1339 1202 1206 5.21 29.091 -2.93 161 NA 161 NA 1090 1347 1209 1214 5.28 29.239 -2.60 162 NA 162 NA 1098 1354 1216 1221 5.56 29.813 -3.00 163 NA 163 NA 1105 1362 1224 1228 5.16 28.984 -2.93 164 NA 164 NA 1112 1369 1232 1236 5.15 28.962 -2.82 165 NA 165 NA 1118 1376 1239 1243 5.19 29.048 -2.68 166 NA 166 NA 1124 1384 1248 1251 5.42 29.53 -3.19 167 NA 167 NA 1130 1392 1255 1258 5.15 28.962 -3.05 168 NA 168 NA 1137 1401 1262 1265 5.24 29.155 -3.10 169 NA 169 NA 1145 1409 1269 1273 5.45 29.591 -2.95 170 NA 170 NA 1151 1416 1277 1280 5.28 29.239 -3.21 171 NA 171 NA 1158 1423 1285 1287 5.33 29.344 -3.06 172 NA 172 NA 1164 1430 1292 1295 4.82 28.226 -3.12 173 NA 173 NA 1170 1438 1300 1302 5.08 28.81 -3.23 174 NA 174 NA 1176 1444 1308 1310 5.25 29.176 -3.08 175 NA 175 NA 1185 1454 1315 1317 5.45 29.591 -3.06 176 NA 176 NA 1192 1461 1323 1324 5.36 29.406 -3.19 177 NA 177 NA 1198 1469 1330 1332 5.54 29.773 -3.07 178 NA 178 NA 1205 1477 1337 1339 5.09 28.832 -3.18 179 NA 179 NA 1210 1484 1345 1347 5.77 30.225 -3.07 180 NA 180 NA 1218 1493 1352 1354 5.24 29.155 -3.09 181 NA 181 NA 1224 1500 1359 1362 5.42 29.53 -3.20 182 NA 182 NA 1232 1509 1368 1369 5.19 29.048 -2.87 183 NA 183 NA 1239 1517 1376 1377 5.35 29.385 -3.14 184 NA 184 NA 1246 1523 1383 1384 5.06 28.766 -3.15 185 NA 185 NA 1254 1531 1390 1392 5.42 29.53 -3.21 186 NA 186 NA 1260 1537 1397 1399 5.24 29.155 -2.92 187 NA 187 NA 1269 1545 1405 1406 5.62 29.932 -3.20 188 NA 188 NA 1277 1553 1412 1414 5.38 29.447 -3.24 189 NA 189 NA 1283 1563 1419 1421 5.40 29.489 -3.20 190 NA 190 NA 1289 1572 1427 1428 5.28 29.239 -3.24 191 NA 191 NA 1296 1579 1436 1436 5.41 29.509 -3.18 192 NA 192 NA 1301 1587 1443 1443 5.25 29.176 -3.19 193 NA 193 NA 1307 1593 1450 1450 5.28 29.239 NA 194 NA 194 NA 1316 1601 1458 1458 5.26 29.197 -3.06 195 NA 195 NA 1323 1610 1466 1466 5.35 29.385 -3.04 196 NA 196 NA 1330 1617 1473 1473 5.42 29.53 -3.20 197 NA 197 NA 1339 1624 1480 1481 5.35 29.385 -3.11 198 NA 198 NA 1344 1632 1488 1488 5.63 29.952 -3.05 199 NA 199 NA 1351 1639 1495 1496 5.16 28.984 -3.05 200 NA 200 NA 1357 1647 1502 1503 5.12 28.897 -2.98 201 NA 201 NA 1365 1656 1510 1511 5.18 29.027 NA